4.7 Article

Exact solutions for steady granular flow in vertical chutes and pipes

Journal

JOURNAL OF FLUID MECHANICS
Volume 930, Issue -, Pages -

Publisher

CAMBRIDGE UNIV PRESS
DOI: 10.1017/jfm.2021.909

Keywords

granular media; rheology; materials processing flows

Funding

  1. Natural Environment Research Council [NE/T010517/1, NE/R011001/1, NE/W004240/1]
  2. Engineering and Physical Sciences Research Council [EP/N025318/1]
  3. Royal Academy of Engineering/The Leverhulme Trust Senior Research Fellowship [LTSRF1617/13/2]
  4. National Natural Science Foundation of China [41831291, 51808401]
  5. China Postdoctoral Science Foundation [2020T130472]
  6. EPSRC [EP/N025318/1] Funding Source: UKRI
  7. NERC [NE/W004240/1, NE/T010517/1, NE/R011001/1] Funding Source: UKRI

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Vertical chutes and pipes play a crucial role in industrial processes involving powders and grains. Through simulations and idealizations, the study reveals linear scaling laws and a novel rheology model for vertical flow, providing insights into the behavior of different flow regimes. The research highlights a linear relation between chute width and shear zone size, contrasting with previous findings and suggesting minimal finite-size effects for the inertial flows studied.
Vertical chutes and pipes are a common component of many industrial apparatus used in the transport and processing of powders and grains. Here, a typical arrangement is considered first in which a hopper at the top feeds the chute and a converging outlet at the bottom controls the mass flux. Discrete element method (DEM) simulations reveal that steady uniform flow is only observed for intermediate flow rates, with jamming and unsteady waves dominating slow flows and non-uniform wall detachment in fast flow. Focusing on the steady uniform regimes, a progressive idealisation is carried out by matching with equivalent DEM simulations in periodic cells. These investigations justify a one-dimensional continuum modelling of the problem and provide key test data. Novel exact solutions are derived here for vertical flow using a linear version of the 'mu(I), Phi(I)-rheology', for which the bulk friction mu and steady solid volume fraction Phi depend on the inertial number I. Despite not capturing the full nonlinear complexities, the solutions match important aspects of the DEM flow fields and reveal simple scaling laws linking many quantities of interest. In particular, this study clearly demonstrates a linear relation between the chute width and the size of the shear zones at the walls. This finding contrasts with previous works on purely quasi-static flow, which instead predict a roughly constant shear zone width, a difference which implies that finite-size effects are minimal for the inertial flows studied here.

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